Paleomagnetic poles and polarity zonation from Cambrian and Devonian strata of Arizona
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Abstract
Basal Paleozoic Tapeats Sandstone (Early and Middle Cambrian) in northern and central Arizona exhibits mixed polarity and a low-latitude paleomagnetic pole. Carbonates of Middle and early Late Cambrian age, and directly superposed carbonate and carbonate-cemented strata of latest Middle(?) and early Late Devonian age, are characterized by reversed polarity and high-latitude poles. The high-latitude Middle Cambrian pole, which appears to record a large but brief excursion of the polar wandering path, is considered provisional pending additional work. The Devonian data from Arizona indicate that a shift of the pole to a “late Paleozoic” position had occurred by Middle Devonian time.
Study Area
Publication type | Article |
---|---|
Publication Subtype | Journal Article |
Title | Paleomagnetic poles and polarity zonation from Cambrian and Devonian strata of Arizona |
Series title | Earth and Planetary Science Letters |
DOI | 10.1016/0012-821X(77)90067-X |
Volume | 36 |
Issue | 3 |
Year Published | 1977 |
Language | English |
Publisher | Elsevier |
Description | 11 p. |
First page | 423 |
Last page | 433 |
Country | United States |
State | Arizona |
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